INSOLATION - определение. Что такое INSOLATION
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Что (кто) такое INSOLATION - определение

POWER PER UNIT AREA RECEIVED FROM THE SUN IN THE FORM OF ELECTROMAGNETIC RADIATION
Solar radiation; Insolation; Solar Radiation; Solar radiance; Solar irradiation; Solar insolation; Solar incidence; Earth's insolation; Solar flux; Total solar irradiance; Total Solar Irradiance; Global insolation; Horizontal irradiation; Global Horizontal Irradiance; Solar potential
  • Insolation variation by month; 1984–1993 averages for January (top) and April (bottom)
  • The shield effect of Earth's atmosphere on solar irradiation. The top image is the annual mean solar irradiation (or insolation) at the top of [[Earth's atmosphere]] (TOA); the bottom image shows the annual insolation reaching the Earth's surface after passing through the atmosphere. The two images use the same color scale.
  • <math>\overline{Q}^\text{day}</math>, the theoretical daily-average irradiation at the top of the atmosphere, where θ is the polar angle of the Earth's orbit, and θ&nbsp;=&nbsp;0 at the vernal equinox, and θ&nbsp;=&nbsp;90° at the summer solstice; φ is the latitude of the Earth. The calculation assumed conditions appropriate for 2000{{nbsp}}A.D.: a solar constant of ''S''<sub>0</sub>&nbsp;=&nbsp;1367&nbsp;W{{nnbsp}}m<sup>−2</sup>, obliquity of ε&nbsp;=&nbsp;23.4398°, longitude of perihelion of ϖ&nbsp;=&nbsp;282.895°, eccentricity ''e''&nbsp;=&nbsp;0.016704. Contour labels (green) are in units of&nbsp;W{{nnbsp}}m<sup>−2</sup>.
  • Variations in Earth's orbit, resulting changes in solar energy flux at high latitude, and the observed glacial cycles.
  • Global distribution of incoming shortwave solar radiation averaged over the years 1981-2010 from the CHELSA-BIOCLIM+ data set<ref>Brun, P., Zimmermann, N.E., Hari, C., Pellissier, L., Karger, D.N. (preprint): Global climate-related predictors at kilometre resolution for the past and future. Earth Syst. Sci. Data Discuss. https://doi.org/10.5194/essd-2022-212</ref>
  • A [[pyranometer]], used to measure global irradiance
  • oblique]] sunbeam distributes its light energy over twice as much area.
  • Spherical triangle for application of the spherical law of cosines for the calculation the solar zenith angle Θ for observer at [[latitude]] φ and [[longitude]] λ from knowledge of the hour angle h and solar declination δ. (δ is latitude of subsolar point, and h is relative longitude of subsolar point).
  • [[Sunlight]] carries radiant energy in the wavelengths of [[visible light]]. Radiant energy may be developed for [[solar power]] generation.
  • Solar irradiance spectrum above atmosphere and at surface
  • Global Map of Direct Normal Radiation <ref name= "Global Solar Atlas" />
  • Global Map of Global Horizontal Radiation <ref name="Global Solar Atlas">World Bank. 2017. Global Solar Atlas. https://globalsolaratlas.info</ref>

insolation         
[??ns?'le??(?)n]
¦ noun technical exposure to the sun's rays.
?the amount of solar radiation reaching a given area.
Origin
C17: from L. insolatio(n-), from insolare, from in- 'towards' + sol 'sun'.
insolation         
n.
1.
Exposure to the rays of the sun.
2.
Drying in the sun.
3.
Sun-stroke, siriasis, coup-de-soleil.
Insolation         
·noun A Sunstroke.
II. Insolation ·noun Exposure of a patient to the sun's rays; a sun bath.
III. Insolation ·noun The act or process to exposing to the rays of the sun fro the purpose of drying or maturing, as fruits, drugs, ·etc., or of rendering acid, as vinegar.

Википедия

Solar irradiance

Solar irradiance is the power per unit area (surface power density) received from the Sun in the form of electromagnetic radiation in the wavelength range of the measuring instrument. Solar irradiance is measured in watts per square metre (W/m2) in SI units.

Solar irradiance is often integrated over a given time period in order to report the radiant energy emitted into the surrounding environment (joule per square metre, J/m2) during that time period. This integrated solar irradiance is called solar irradiation, solar exposure, solar insolation, or insolation.

Irradiance may be measured in space or at the Earth's surface after atmospheric absorption and scattering. Irradiance in space is a function of distance from the Sun, the solar cycle, and cross-cycle changes. Irradiance on the Earth's surface additionally depends on the tilt of the measuring surface, the height of the Sun above the horizon, and atmospheric conditions. Solar irradiance affects plant metabolism and animal behavior.

The study and measurement of solar irradiance have several important applications, including the prediction of energy generation from solar power plants, the heating and cooling loads of buildings, climate modeling and weather forecasting, passive daytime radiative cooling applications, and space travel.